Study on the Distribution Regularity of OilWater and Main Controlling Factors in Hujianshan Area,Ordos Basin
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摘要: 利用岩芯、录井和测井等基础资料,对胡尖山地区长6段地层沉积相演化特征进行了研究,分析了油水层的分布规律及控制油水层相间分布的地质条件。胡尖山地区砂体微相主要包括水下分流河道、河口坝、远砂坝、河道间四种类型,勘探成果表明不同沉积微相均有油藏分布,厚层叠置砂体多为水层占据, 同一时期沉积砂体的不同部位含油性不尽相同。研究区油水的这种复杂分布特征说明沉积相不是控制油水复杂分布的唯一因素。储层内部结构、钙质胶结程度、原油侧向输导能力及不同时期沉积砂体的连通性都对油水层的分布起到一定的控制作用。其中,沉积微相砂体展布特征、原油侧向输导能力及储层内部结构是制约油水分布的主要原因。Abstract: Based on the fundamental data of core, log and well logging,we studied the sedimentary microfacies types and evolutionary feature of Chang 6 in Hujianshan area and analyzed the distribution regular pattern of the oil and water and geologic condition which controlled the distribution of oil and water layers. The result showed there were four sandmicrofacies in Hujianshan area,including the subaqueous distributary channel, channelmouth bar, distal bar and interdistributary. The schedule of exploration indicates that oil reservoir can be found in different sedimentary microfacies and water layer almost seize thicklystratified sand. Oilbearing capability of different parts of sedarenite deposited at the same time is not exactly the same. The complex character about distribution regularity of oil and water shows that sedimentary facies are not the unique factor which controls the complicate distribution of oil and water. Internal reservoir structure ,calcarinate degree,the capability of oil lateral migration and the connectivity of sedarenite in different periods all had an effect on distribution regularity of oil and water, but the important reasons were the sand distribution feature,the capability of oil lateral migration and internal reservoir structure.
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